Name: LaPaz Icefield 04757 This is an OFFICIAL meteorite name. Abbreviation: LAP 04757 Observed fall: No Year found: 2004 Country: Antarctica [Collected by US Antarctic Search for Meteorites program (ANSMET)] Mass: 12.8 g
Macroscopic Description: Kathleen McBride Exteriors of these meteorites have dull brown/black fusion crust with oxidation haloes. The interiors reveal a rusty brown/black matrix with high metal content.
Thin Section (,2) Description: Tim McCoy and Valerie Reynolds These meteorites are so similar that a single description suffices. The sections consist of abundant chondrules set in a metal- and sulfide-bearing, weathered matrix. Shock effects are present, including metal-sulfide melting at grain boundaries. Olivine is homogeneous at Fa13 and pyroxene exhibits a small range at Fs13-16. Links to the acapulcoites or low-FeO chondrites (Russell et al., 1998) should be considered, although LAP 04773/04757 are less metamorphosed than the former and more magnesian than is typical for the latter.
Russell S.S., McCoy T.J., Jarosewich E., and Ash R.D. (1998) The Burnwell, Kentucky, low iron oxide chondrite fall: Description, classification and origin. Meteorit. Planet. Sci.33, 853-856. (link)